2013
DOI: 10.1016/j.nrjag.2013.12.003
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Gravity observations at Sinai Peninsula and its geophysical and geodetic applications

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Cited by 4 publications
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“…The Peninsula of Sinai is divided into three geological districts, namely, the granitic and metamorphic mountains, the limestone plateaus, and the sandstone coastal plain. The structural elements of the Sinai Peninsula are strongly dominated by its active boundaries due to its location at the triple junction among the Gulf of Suez rift, the Aqaba-Levant transform fault, and the Red Sea Rift [31]. Two major fault systems played a principal role in creating the geomorphology of the Sinai Peninsula; these are the Sinai Hing Belt (Minsherah-Abu Kandu shear zone) and the Themed Fault (Ragabet El-Naam fault) (Fig.…”
Section: Geo-tectonicmentioning
confidence: 99%
“…The Peninsula of Sinai is divided into three geological districts, namely, the granitic and metamorphic mountains, the limestone plateaus, and the sandstone coastal plain. The structural elements of the Sinai Peninsula are strongly dominated by its active boundaries due to its location at the triple junction among the Gulf of Suez rift, the Aqaba-Levant transform fault, and the Red Sea Rift [31]. Two major fault systems played a principal role in creating the geomorphology of the Sinai Peninsula; these are the Sinai Hing Belt (Minsherah-Abu Kandu shear zone) and the Themed Fault (Ragabet El-Naam fault) (Fig.…”
Section: Geo-tectonicmentioning
confidence: 99%